An Analysis of Swarm Earthquakes in the Area of the Elbrus Volcanic Center

Dudarov, Z. I.; Dmitrieva, I. Yu.; Sayapina, A. A.; Bagaeva, S. S.

doi:10.1134/s0742046323700367

Cited by 1 publication

(1 citation statement)

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“…It is covered by extensive glaciers (>100 km 2 ). The geology and natural environment of this mountain have been studied for a long time, and contemporary knowledge can be found, particularly, in the works by Bindeman et al [62], Dubinina et al [63], Dudarov et al [64], Holobâcǎ [65], Koronovskii et al [66], Koronovsky and Myshenkova [67], Kutuzov et al [68], Lebedev et al [69], Milyukov and Myasnikov [70], Milyukov et al [71], and Rogozhin et al [72]. The Elbrus is an emblematic mountain of the Russian South.…”

Section: Little Saddlementioning

confidence: 99%

Geoheritage Value of Three Localities from Kislovodsk in the Southern Central Ciscaucasus: A Resource of Large Resort Area

Yashalova,

Ruban

2024

Geosciences

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Many geographical domains possess notable geological and geomorphological features, which are yet to be characterized comprehensively in terms of geoheritage. The present study focuses on the Kislovodsk area, which is situated in the southern part of the Central Ciscaucasus (post-Paleozoic platform), where the latter joins to the Greater Caucasus (late Cenozoic orogen). Three geosites are reported from there, and their qualitative description and semi-quantitative, score-based assessment are offered. The Honey Waterfalls represent an example of river erosion affecting Carboniferous granitoids with uppermost Jurassic weathering horizon and overlain by Lower Cretaceous carbonates. The Ring Mountain is a natural arch formed as result of wind erosion. The Little Saddle is a viewpoint offering a spectacular, panoramic view toward the Elbrus Mountain that is the highest peak of Russia and Europe and an impressive dormant stratovolcano. The Honey Waterfalls and the Ring Mountain are ranked nationally (the latter receives the highest total scores), and the Little Saddle is ranked regionally. These geosites are diverse in several aspects, and, particularly, different geoheritage types and forms are established. The Kislovodsk area bearing the reported geoheritage objects is a part of the Mineralnye Vody resort area, which is large and important for the national tourism and recreation industry. The related opportunities and challenges for geoheritage resource management have to be considered.

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